RZ

Revolver Resources Inc. (TSX VENTURE:RZ) is pleased to present a new 3D IP model
based upon the results of the IP (resistivity/chargeability) survey carried out
on its Summit B property located in the Iskut area of northwestern British
Columbia, Canada. The model reveals a strong 2.0 km long-500 m wide, NW-oriented
ovoid chargeability anomaly with values reaching over 35 mV/V accompanied by low
resistivity signatures (see Figure 1). It extends from shallow depth (less than
100 m) to at least 500 m and is open at both the NW and SE ends. Surface geology
indicates the high chargeability/low resistivity anomaly is spatially related to
Cu-Au bearing disseminated sulphide bodies and stockworks distributed within
fault zones. Recent rock and chip sampling of historic mineralized trenches
generated substantial Cu assay values ranging from 0.1 to 1.5 wt. %. Gold is
significantly enriched, highlighted by several concentrations greater than 3 g/t
Au; i.e. 3.0 g/t, 17.9 g/t, 12.3 g/t, 10.9 g/t. Pervasive
hematite-ankerite-silica alteration affected the sheared volcanosedimentary
rocks. Revolver Resources intends to initially test the anomaly by conducting a
1,000 m drilling campaign. 


The Summit B IP anomaly is similar in shape and intensity to that observed in
Colorado Resources adjacent North Rok property. The North Rok chargeability
anomalies characterized a porphyry copper-gold system associated with an Early
Jurassic monzodiorite-diorite pluton intruding Upper Triassic Stuhini Group
volcanic rocks. Already, drill core intersections of 402 m @ 0.28 wt. % Cu and
0.27 g/t and 242 m @ 0.63 wt. % Cu and 0.85 g/t Au were obtained less than 3 km
away from Revolver's property. The Summit B IP anomaly is associated with low
magnetic values relative and occur in a greenschist metamorphosed
Mississippian-Permian volcanosedimentary assemblage. The age of the Summit B
mineralization is presumed to be Jurassic and concordant with the age of alkalic
intrusions at North Rok, Red Chris (a porphyry copper-gold mine and with
reserves of over 300 million tonnes grading 0.359% copper and 0.274 g/t gold)
and elsewhere in northwestern BC. The carbonate alteration and precious metal
mineralization at Summit B may be related to deep metamorphic fluids with
appropriate chemistry to cause quartz-carbonate-gold deposits. Alternatively,
the mineralization may be produced by hydrothermal fluids generated by the
intrusion of alkalic plutonic rocks at moderate depth. 


To view Figure 1, please visit the following link:
http://media3.marketwire.com/docs/rz1108-F1.pdf.


Technical information in this news release has been prepared and/or revised by
Michel Boily, PhD, P.Geo, and Qualified person as defined in NI 43-101. 


For further information on Revolver and the 3D IP model please visit our website
at www.revolverresources.com. 


ON BEHALF OF THE BOARD OF DIRECTORS 

Robert L. Birmingham, President 

NEITHER TSX VENTURE EXCHANGE NOR ITS REGULATION SERVICE PROVIDER (AS THAT TERM
IS DEFINED IN THE POLICIES OF THE TSX VENTURE EXCHANGE) ACCEPTS RESPONSIBILITY
FOR THE ADEQUACY OR ACCURACY OF THIS RELEASE.


FOR FURTHER INFORMATION PLEASE CONTACT: 
Revolver Resources Inc.
Robert Birmingham
(778) 331-2025
(604) 683-5309 (FAX)
rob@revolverresources.com
www.revolverresources.com

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